Probing discontinuous precipitation in U-Nb

Abstract

U-Nb's discontinuous precipitation, γbccmatrix → αorthcellular + γ'bcccellular, is intriguing in the sense that it allows formation and growth of the metastable γ' phase during the course of its occurrence. Previous attempts to explain the thermodynamic origin of U-Nb's discontinuous precipitation hypothesized that the energy of α forms an intermediate common tangent with the first potential of the double-well energy of γ at the γ' composition. While this hypothesis is eligible and consistent with the experimental observation of gradual increase in γ' composition at increasing temperature, it is in conflict with recent experiments whose results indicated a distribution of γ' compositions in the vicinity of 50 at\%Nb. To shed some light onto this issue, the current work investigates the origin of U-Nb's discontinuous precipitation in view of fundamental thermodynamics and kinetics, taken from the perspective of phase-field theory. It has been showed that local misfit strain tends to play a crucial role in the formation and growth the discontinuous precipitation. Depending on the magnitude of strain developed at grain boundaries, either an increasing γ' composition or a random distribution of γ' composition around the equiatomic value with respect to increasing temperature could be expected.

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